% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17360 % Primary Name: FISHERMANS LAKE LIBERIA % Record Type: TAVG % Country: Liberia % Latitude: 6.75000 +/- 0.00500 % Longitude: -11.25000 +/- 0.00500 % Elevation (m): 0.00 +/- 0.05 % # of Months: 23 % % IDs: gsod - 749023-99999 % usaf - 749023 % % Sources: Global Summary of the Day % % Site Hash: 762e78ca7db9fc6f95b5073ce4ea3b09 % Raw Data Hash: 490263e462859b44dff66df360044284 % Adj Data Hash: 815f70d8c06ffeaf82530edb214e8a33 % % The data for this station is presented below in several columns and in % several forms. The temperature values are reported as "raw", % "adjusted", and "regional expectation". % % The "raw" values reflect the observations as originally ingested by % the Berkeley Earth system from one or more originating archive(s). % These "raw" values may reflect the merger of more than one temperature % time series if multiple archives reported values for this location. % Alongside the raw data we have also provided a flag indicating which % values failed initial quality control checks. A further column % dates at which the raw data may be subject to continuity "breaks" % due to documented station moves (denoted "1"), prolonged measurement % gaps (denoted "2"), documented time of observation changes (denoted "3") % and other empirically determined inhomogeneities (denoted "4"). % % In many cases, raw temperature data contains a number of artifacts, % caused by issues such as typographical errors, instrumentation changes, % station moves, and urban or agricultural development near the station. % The Berkeley Earth analysis process attempts to identify and estimate % the impact of various kinds of data quality problems by comparing each % time series to neighboring series. At the end of the analysis process, % the "adjusted" data is created as an estimate of what the weather at % this location might have looked like after removing apparent biases. % This "adjusted" data will generally to be free from quality control % issues and be regionally homogeneous. Some users may find this % "adjusted" data that attempts to remove apparent biases more % suitable for their needs, while other users may prefer to work % with raw values. % % Lastly, we have provided a "regional expectation" time series, based % on the Berkeley Earth expected temperatures in the neighborhood of the % station. This incorporates information from as many weather stations as % are available for the local region surrounding this location. Note % that the regional expectation may be a systematically a bit warmer or % colder than the weather stations by a few degrees due to differences % in mean elevation and other local characteristics. % % For each temperature time series, we have also included an "anomaly" % time series that removes both the seasonality and the long-term mean. % These anomalies may provide an easier way of seeing changes through % time. % % Reported temperatures are in Celsius and reflect monthly averages. As % these files are intended to be summaries for convenience, additional % information, including more detailed flagging and metadata, may be % available in our whole data set files. % % The Berkeley Earth analysis was run on 15-Nov-2013 19:55:48 % % Raw Data QC Continuity Adjusted Data Regional Expectation % Year, Month, Temperature, Anomaly, Failed, Breaks, Temperature, Anomaly, Temperature, Anomaly 1942 7 NaN NaN NaN NaN NaN NaN 23.987 -0.574 1942 8 NaN NaN NaN NaN NaN NaN 23.934 -0.493 1942 9 NaN NaN NaN NaN NaN NaN 25.481 0.349 1942 10 NaN NaN NaN NaN NaN NaN 25.540 -0.070 1942 11 NaN NaN NaN NaN NaN NaN 26.214 0.290 1942 12 NaN NaN NaN NaN NaN NaN 24.909 -0.372 1943 1 NaN NaN NaN NaN NaN NaN 25.382 -0.305 1943 2 NaN NaN NaN NaN NaN NaN 26.335 -0.525 1943 3 NaN NaN NaN NaN NaN NaN 26.936 -0.349 1943 4 NaN NaN NaN NaN NaN NaN 26.618 -0.367 1943 5 NaN NaN NaN NaN NaN NaN 26.632 0.032 1943 6 NaN NaN NaN NaN NaN NaN 25.357 -0.186 1943 7 25.081 -0.253 0 0 25.081 -0.253 24.148 -0.413 1943 8 24.600 -0.599 0 0 24.600 -0.599 23.970 -0.456 1943 9 25.320 -0.584 0 0 25.320 -0.584 24.843 -0.289 1943 10 26.222 -0.161 0 0 26.222 -0.161 25.161 -0.450 1943 11 27.102 0.406 0 0 27.102 0.406 26.006 0.083 1943 12 26.457 0.404 0 0 26.457 0.404 25.095 -0.186 1944 1 26.423 -0.037 0 0 26.423 -0.037 25.360 -0.327 1944 2 26.952 -0.680 0 0 26.952 -0.680 26.877 0.017 1944 3 27.461 -0.597 0 0 27.461 -0.597 26.995 -0.290 1944 4 27.748 -0.009 0 0 27.748 -0.009 26.939 -0.046 1944 5 28.131 0.758 0 0 28.131 0.758 27.139 0.538 1944 6 26.744 0.429 0 0 26.744 0.429 25.699 0.156 1944 7 25.314 -0.020 0 0 25.314 -0.020 24.380 -0.182 1944 8 24.821 -0.378 0 0 24.821 -0.378 24.280 -0.147 1944 9 25.521 -0.383 0 0 25.521 -0.383 25.152 0.020 1944 10 26.414 0.031 0 0 26.414 0.031 25.656 0.045 1944 11 27.006 0.310 0 0 27.006 0.310 26.373 0.450 1944 12 26.909 0.855 0 0 26.909 0.855 25.628 0.347 1945 1 26.950 0.490 0 0 26.950 0.490 26.196 0.508 1945 2 27.581 -0.051 0 0 27.581 -0.051 27.186 0.326 1945 3 28.109 0.052 0 0 28.109 0.052 27.653 0.368 1945 4 28.120 0.363 0 0 28.120 0.363 27.260 0.275 1945 5 27.408 0.035 1 0 NaN NaN 26.794 0.193 1945 6 NaN NaN NaN NaN NaN NaN 25.981 0.438 1945 7 NaN NaN NaN NaN NaN NaN 24.220 -0.341 1945 8 NaN NaN NaN NaN NaN NaN 24.092 -0.335 1945 9 NaN NaN NaN NaN NaN NaN 25.220 0.088 1945 10 NaN NaN NaN NaN NaN NaN 25.586 -0.025 1945 11 NaN NaN NaN NaN NaN NaN 26.512 0.589 1945 12 NaN NaN NaN NaN NaN NaN 25.432 0.151 1946 1 NaN NaN NaN NaN NaN NaN 25.853 0.166 1946 2 NaN NaN NaN NaN NaN NaN 27.206 0.347 1946 3 NaN NaN NaN NaN NaN NaN 27.601 0.316 1946 4 NaN NaN NaN NaN NaN NaN 27.151 0.167 1946 5 NaN NaN NaN NaN NaN NaN 26.635 0.034